Recent Decline in Antarctic Sea Ice Cover From 2016 to 2022: Insights From Satellite Observations, Argo Floats, and Model Reanalysis

• Published in: Tellus A: Dynamic Meteorology and Oceanography
• Main Authors: Suryawanshi, Kshitija, Jena, B., Bajish, C. C., Anilkumar, N.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Stockholm University Press 2023
• Subjects: Antarctic; Antarctic Peninsula; Pacific; Southern Ocean; Antarc*; Sea ice
• Online Access: http://dx.doi.org/10.16993/tellusa.3222; https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3222/6384; https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3222/6385; https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3222/6386

Ever since the abrupt drop in Antarctic sea ice extent (SIE) began in spring of 2016, as opposed to its consistent growth (1.95% decade–1 from 1979 to 2015), the SIE in the satellite era has reached record lows in 2017 and 2022. From spring 2016, the satellite-based SIE remained consistently lower than the long-term mean, with the trend dropping to 0.11% decade–1 from 1979 to 2022. The top record lowest SIE years were observed from 2016 to 2022, corresponding to the warmest years dating back to 1979. With this background, the rare features of Antarctic polynyas reoccurred frequently and the west Antarctic Peninsula remained ice-free throughout 2022. Recently, the SIE dropped to a record low in June 2022, July 2022, August 2022, January 2023, and February 2023, which were 13.67%, 9.91%, 6.79%, 39.29%, 39.56% below the long-term mean value, respectively for months described above. We find that the observed decline in SIE during 2016–2022 occurred due to the combined influences from the intensification of atmospheric zonal waves with enhanced poleward transport of warm-moist air and anomalous warming in the Southern Ocean mixed layer (>1°C). Although the sudden sea ice decline in spring of 2016 occurred corresponding to the transitional climate shift from IPO– (Interdecadal Pacific Oscillation, 2000–2014) to IPO+ (2014–2016), the recent decline after 2016 occurred in a dominant IPO– and Southern Annular Mode (SAM+). CMIP6 models showed a consistent decrease in ensemble-mean SIE from 1979 to 2022. The model trend exhibits similarities to the recent declining trend in SIE from satellite observations since 2016, suggesting a possible shift towards a warmer climatic regime.